31.03.2014 Views

Computer simulation of thermal convection in Rayleigh-Bénard cell ...

Computer simulation of thermal convection in Rayleigh-Bénard cell ...

Computer simulation of thermal convection in Rayleigh-Bénard cell ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Hubert Jopek<br />

<strong>Computer</strong> <strong>simulation</strong> <strong>of</strong> <strong>thermal</strong> <strong>convection</strong> <strong>in</strong> <strong>Rayleigh</strong>-<strong>Bénard</strong> <strong>cell</strong><br />

Chapter 3: Description <strong>of</strong> the geometry <strong>in</strong> <strong>Rayleigh</strong>-<strong>Bénard</strong> model<br />

The Geometry <strong>of</strong> the <strong>Rayleigh</strong>-<strong>Bénard</strong> model is presented below:<br />

Fig. 3.1: The fluid layer model.<br />

the top<br />

The model is a very long narrow fluid layer. There are fixed temperatures at<br />

T<br />

C<br />

and at the bottom<br />

Tw<br />

and the temperature at the bottom is higher so<br />

T<br />

w<br />

> T c<br />

. The difference <strong>of</strong> the temperature is expressed by the term δT<br />

= T w<br />

−Tc<br />

this is one <strong>of</strong> the control parameters <strong>of</strong> the system. Convection appears when the<br />

temperature gradient is big enough, consequently a small packet <strong>of</strong> fluid starts to<br />

move up <strong>in</strong>to the colder region <strong>of</strong> higher density. If the buoyant force caused by<br />

difference <strong>of</strong> density is big enough, then the pocket moves upward so fast that the<br />

temperature cannot drop and the convective flow appears. There is also possible<br />

that the buoyant force is not strong enough, <strong>in</strong> such a situation the temperature <strong>of</strong><br />

the pocket is able to drop before it can move up too much, and as a result fluid stays<br />

stable.<br />

and<br />

Fig. 3.2: Transition from <strong>thermal</strong> conduction to convective rolls <strong>in</strong> <strong>in</strong>f<strong>in</strong>ite twodimensional<br />

fluid layer.<br />

8

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!